ZHANG Hua, JING Wenbo, TANG Xinping, WANG Yu, WANG Gang, XU Xiongfei
The eastern slope of Tiancao Sag is rich in oil and gas resources in the second Member of Cretaceous Bayingebi Formation,but faces challenges including rapid reservoir lateral changes and unclear developmental control factors,which constrain the hydrocarbon reservoir exploration progress in this area. Therefore,adopting a structure-sedimentation coupling research approach and integrating technical methods such as seismic interpretation,paleogeomorphology restoration,core observation,thin section identification,and log facies analysis,this study systematically investigated the structural characteristics,sedimentary reservoir distribution patterns,and their coupling relationships on the eastern slope. The results are obtained in three aspects. (1)The eastern slope of Tiancao Sag develops major long-term active faults that control sedimentation,which continuously move with tectonic activities, forming fault slope-break belts. These fault slope-break belts significantly control sedimentation,resulting in steeper topography near the slope-break belts and abrupt changes in stratum thickness on both sides of the slope-break. (2)During the sedimentary period of the second Member of Bayingebi Formation,the main sedimentary facies on the eastern slope was braided river delta front,which can be further divided into two facies belts of inner-front and outer-front. The delta inner-front facies belts is closer to the provenance,with faster sedimentation rate,poorer rock sorting,and inferior porosity-permeability conditions. The delta outer-front facies belt is relatively farther from the provenance,where sediments are more strongly modified by lake water,with better sandstone sorting,favorable for pore development and connectivity,and better porosity-permeability conditions. (3)Overlay analysis of fault slope-break belts and sedimentary facies shows significant differences in sedimentary microfacies on both sides of the fault slope-break belts. The fault slope-break belts precisely serve as the boundary between inner and outer fronts. Above the fault slope-break belts,the delta inner-front facies belt mainly develops,with sedimentary microfacies primarily being underwater distributary channels, characterized by coarser lithology,poorer sorting,and inferior physical properties. Below the fault slope-break belts,the delta outer-front facies belt mainly develops,with sedimentary microfacies primarily being underwater distributary channels and mouth bars,characterized by finer lithology,better sorting,and better physical properties,making it a favorable reservoir development area. The research findings provide theoretical basis and practical reference for hydrocarbon reservoir exploration in Tiancao Sag and similar geological conditions areas.